The Exceptionally Warm Winter of 2015/16 in Alaska

• Published in: Journal of climate Vol. 30; no. 6; pp. 2069 - 2088
• Main Authors: Walsh, John E., Bieniek, Peter A., Brettschneider, Brian, Euskirchen, Eugénie S., Lader, Rick, Thoman, Richard L.
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 01.03.2017
• Subjects: Air pollution; Albedo; Albedo (solar); Albedo effects; Analogs; Anomalies; Assimilation; Atmospheric circulation; Atmospheric models; Biology; Boreal forests; Circulation; Climate; Climate change; Climate models; Climate science; Cold; Cold season; Computer simulation; Dynamic height; Gases; Geopotential; Geopotential height; Greenhouse effect; Greenhouse gases; Ice cover; Ocean surface; Ocean temperature; Precipitation; Sea ice; Sea level; Sea level pressure; Seasons; Snow; Snow cover; Snowpack; Spring; Surface temperature; Temperature; Temperature (air-sea); Trends; Tundra; Winter; Arctic Ocean
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/jcli-d-16-0473.1

Alaska experienced record-setting warmth during the 2015/16 cold season (October–April). Statewide average temperatures exceeded the period-of-record mean by more than 4°C over the 7-month cold season and by more than 6°C over the 4-month late-winter period, January–April. The record warmth raises two questions: 1) Why was Alaska so warm during the 2015/16 cold season? 2) At what point in the future might this warmth become typical if greenhouse warming continues? On the basis of circulation analogs computed from sea level pressure and 850-hPa geopotential height fields, the atmospheric circulation explains less than half of the anomalous warmth. The warming signal forced by greenhouse gases in climate models accounts for about 1°C of the anomalous warmth. A factor that is consistent with the seasonal and spatial patterns of the warmth is the anomalous surface state. The surface anomalies include 1) above-normal ocean surface temperatures and below-normal sea ice coverage in the surrounding seas from which air advects into Alaska and 2) the deficient snowpack over Alaska itself. The location of the maximum of anomalous warmth over Alaska and the late-winter–early-spring increase of the anomalous warmth unexplained by the atmospheric circulation implicates snow cover and its albedo effect, which is supported by observational measurements in the boreal forest and tundra biomes. Climate model simulations indicate that warmth of this magnitude will become the norm by the 2050s if greenhouse gas emissions follow their present scenario.